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辽北西丰地区宝兴岩体LA-ICP-MS锆石U-Pb年龄及岩石地球化学特征

彭游博 宋淑娥 刘锦 张文静 王恩德 赵辰

地质通报2017,Vol.36Issue(10):1698-1707,10.
地质通报2017,Vol.36Issue(10):1698-1707,10.

辽北西丰地区宝兴岩体LA-ICP-MS锆石U-Pb年龄及岩石地球化学特征

LA-ICP-MS zircon U-Pb dating and geochemical characteris-tics of Baoxing rock mass in Xifeng area of northern Liaoning Province

彭游博 1宋淑娥 2刘锦 3张文静 1王恩德 4赵辰5

作者信息

  • 1. 辽宁省地质矿产调查院,辽宁沈阳110031
  • 2. 东北大学资源与土木工程学院,辽宁沈阳110004
  • 3. 辽宁省地质实验研究所,辽宁沈阳110032
  • 4. 吉林大学地球科学学院,吉林长春130000
  • 5. 辽宁省地震局,辽宁沈阳110034
  • 折叠

摘要

Abstract

Located on the northern margin of North China Block, the Baoxing rock mass is mainly composed of granodiorite. Ac-cording to LA-ICP-MS zircon U-Pb dating, it was formed in Middle Triassic, with the 206Pb/238U age of 235.0±1.3Ma. The aver-age K2O/Na2O ratio is 1.07, indicating that the rocks belong to high-K calc-alkaline series. The rocks are enriched in LILE and de-pleted in HFSE, showing typical features of calc-alkaline series on an active continental margin. The average total amount of REE is 147×10-6, and the curve exhibits obvious right-inclined feature on REE distribution pattern, suggesting that the rocks are of the type of LREE enrichment and HREE depletion with medium negative Eu anomaly. According to the petrology, geochemistry and geo-chronology in combination with the tectonic evolution research on adjacent areas, lithospheric delamination occurred under the ex-tension in the study area, and then caused a large-scale magmatic activity in the Middle Triassic.

关键词

中三叠世/LA-ICP-MS锆石U-Pb测年/宝兴岩体/花岗闪长岩/辽北地区/华北板块

Key words

Middle Triassic/LA-ICP-MS zircon U-Pb dating/Baoxing rock mass/granodiorite/northern Liaoning Province/North China Block

分类

天文与地球科学

引用本文复制引用

彭游博,宋淑娥,刘锦,张文静,王恩德,赵辰..辽北西丰地区宝兴岩体LA-ICP-MS锆石U-Pb年龄及岩石地球化学特征[J].地质通报,2017,36(10):1698-1707,10.

基金项目

中国地质调查局项目《辽东-吉南成矿带永吉—凤城地区地质矿产调查》(编号:DD20160049) (编号:DD20160049)

地质通报

OA北大核心CSCDCSTPCD

1671-2552

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